A Classical-Theory-Based Parameterization of Heterogeneous Ice Nucleation by Mineral Dust, Soot, and Biological Particles in a Global Climate Model
By C. Hoose, J. Kristjánsson, Jen‐Ping Chen, A. Hazra. 2010
370 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/788117febe44e0f72dbaee3238d6ffc944643d11
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Citations in the corpus
- A New Ice Nucleation Active Site Parameterization for Desert Dust and Soot (2017, methodology): “Parameterizations based on CNT (e.g., Hoose et al. 2010; Chen et al. 2008; Barahona 2012; Savre and Ekman 2015) depend on parameters that are difficult to determine.”
- Aerosol–climate interactions in the Norwegian Earth System Model – NorESM1-M (2012, background): “These are neither discussed in this paper nor currently included in NorESM, although research development is ongoing for later inclusion (Hoose et al., 2010; Storelvmo et al., 2011; see also Gettelman et al., 2010).”
- A comprehensive laboratory study on the immersion freezing behavior of illite NX particles. A comparison of 17 ice nucleation measurement techniques (2014, background): “Among the various modes of atmospheric ice nucleation, immersion freezing is one of the most important mechanisms for primary ice formation, accounting for 85 % of ice formation in clouds that contain supercooled droplets (Hoose et al., 2010).”
- Bacterial abundance and viability in long-range transported dust (2012, background): “Thus information on bacterial abundance and viability is necessary to estimate their influences onpublic health, downwind ecosystems and atmospheric phenomena (Griffin, 2007; Hoose et al., 2010; Ichinose et al., 2008).”
- Intercomparison of the cloud water phase among global climate models (2014, methodology): “Heterogeneous ice nucleation follows a semiempirical parameterization based on classical nucleation theory [Hoose et al., 2010].”
- Improvements to an Empirical Parameterization of Heterogeneous Ice Nucleation and Its Comparison with Observations (2013, background): “Although Hoose et al. (2010) predicted an almost negligible fraction (about 1027) of all active IN that are PBAPs globally, their global model may have greatly underestimated it due to their treatment of bacterial ice nucleation using observations of IN activity of only one strain of Pseudomonas…”
- Opinion: Cloud-phase climate feedback and the importance of ice-nucleating particles (2020, background): “We have begun to build models of the global distribution of atmospheric INPs (Vergara-Temprado et al., 2017; Hoose et al., 2010; Spracklen and Heald, 2014; Schill et al., 2020), but we currently lack an understanding of middle- and high-latitude sources.”
- The adsorption of fungal ice-nucleating proteins on mineral dusts: a terrestrial reservoir of atmospheric ice-nucleating particles (2016, background): “However, number densities of these supermicron biological particles are typically many orders of magnitude lower than those of their inorganic counterparts at altitudes relevant for supercooled clouds (Hoose et al., 2010).”
- Aerosol Mixing State: Measurements, Modeling, and Impacts (2019, background): “3) lends itself to a “type-based approach” of representing ice nucleation, where different ice nucleation propensities are assigned to the various particle types (e.g., dust, biological particles, and soot; Hoose et al., 2010).”